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    Further Analyses of the Climax Cloud-Seeding Experiments

    Source: Journal of Applied Meteorology:;1993:;volume( 032 ):;issue: 012::page 1837
    Author:
    Rangno, A. L.
    ,
    Hobbs, P. V.
    DOI: 10.1175/1520-0450(1993)032<1837:FAOTCC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A further examination of the Climax I and II randomized cloud-seeding experiments has revealed the following. 1) Cloud seeding had no effect on precipitation in Climax I after the control stations had been chosen halfway through the experiment. 2) Faulty execution of the randomization scheme resulted in a misleading precipitation climatology and a misleading relationship between cloud-top and 500-mb temperatures for the control days. 3) The method of assigning upper-level winds and temperatures to experimental days emphasized widespread, synoptic-scale weather systems with cloud tops far above 500 mb rather than the orographic ?blanket? clouds that were sought. 4) Particle trajectory calculations show that it is unlikely that the silver iodide released from the ground could have affected precipitation at Climax in southwest flow, the category for which the greatest seeding effect was reported.
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      Further Analyses of the Climax Cloud-Seeding Experiments

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4147276
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    contributor authorRangno, A. L.
    contributor authorHobbs, P. V.
    date accessioned2017-06-09T14:04:41Z
    date available2017-06-09T14:04:41Z
    date copyright1993/12/01
    date issued1993
    identifier issn0894-8763
    identifier otherams-11988.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147276
    description abstractA further examination of the Climax I and II randomized cloud-seeding experiments has revealed the following. 1) Cloud seeding had no effect on precipitation in Climax I after the control stations had been chosen halfway through the experiment. 2) Faulty execution of the randomization scheme resulted in a misleading precipitation climatology and a misleading relationship between cloud-top and 500-mb temperatures for the control days. 3) The method of assigning upper-level winds and temperatures to experimental days emphasized widespread, synoptic-scale weather systems with cloud tops far above 500 mb rather than the orographic ?blanket? clouds that were sought. 4) Particle trajectory calculations show that it is unlikely that the silver iodide released from the ground could have affected precipitation at Climax in southwest flow, the category for which the greatest seeding effect was reported.
    publisherAmerican Meteorological Society
    titleFurther Analyses of the Climax Cloud-Seeding Experiments
    typeJournal Paper
    journal volume32
    journal issue12
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1993)032<1837:FAOTCC>2.0.CO;2
    journal fristpage1837
    journal lastpage1847
    treeJournal of Applied Meteorology:;1993:;volume( 032 ):;issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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